Blar i Artikler på emneord "FYLLITT"

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    • Foreløpige meddelelser fra kartbladet Essandsjø. 

      Bjørlykke, Unni (NGU (223), Journal article, 1963)
      A symposis is given of 4-5 weeks of field work in the Sylene area, Sør-Trøndelag, Norway, in the eastern part of the Cambro-Silurian geosyncline of Trondhjemsfeltet. Previous investigations are reffered to. The rocks in ...

    • Grensen fyllitt - Valdres-sparagmitt i strøket sydøst for Grønsennknipa, Vestre Slidre. 

      Holtedahl, Olaf (NGU (213), Journal article, 1961)
      In a paper of 1959 the writer described boundaries between the Ordovician \"phyllite formation\" and the overlying \"Valdres Sparagmite\" in and just east of the Grønsennknipa mountain mass, west of the Valdres valley, and ...

    • Kartbladet Lillehammer. Tekst 

      Munster, Ths. (NGU (30), Journal article, 1900)
      Forkortet: Diese Abhandlung enthalt eine Beschreibung des geologischen Kartenblattes \"Lillehammer\" (Zwischen 60\u00B0 54' und 61\u00B0 1' N und zwischen ca. 0\u00B0 2' und 0\u00B0 48' west. Lange von Oslo Observatorium). ...

    • Kisdistriktet Varaldsøy-Ølve i Hardanger og bergverksdriftens historie. 

      Foslie, Steinar; Dietrichson, Brynjulf (NGU (147), Journal article, 1955)
      When Steinar Foslie suddenly passed away in november 1951, he had finished the geological map here presented: \"Kisdistriktet Varaldsøy-Ølve i Hardanger\", based on field-work during 1942-49. Furthermore his M.S. contained ...

    • On kink-zone development and metamorphic differentiation in the low-grade schists of Norwegian Sulitjelma. 

      Nicholson, Robin (NGU (247), Journal article, 1967)
      The common minor scale kink-zones of upper levels of the Furulund schists of eastern Norwegian Sulitjelma generally do not occur in conjugate pairs: usually only the member with northwest dipping axial plane is developed ...

    • Valdres-sparagmittens stratigrafiske stilling. 

      Strand, Trygve (NGU (205), Journal article, 1959)
      The Valdres Sparagmite is a deposit chiefly of arkoses (sparagmites) in central Southern Norway. It lies above fossiliferous Ordovician sediments and has thus been considered as of Ordovician or Silurian age by Norwegian ...